Decadal changes in Atlantic overturning due to the excessive 1990s Labrador Sea convection

Abstract Changes in the Atlantic Meridional Overturning Circulation (AMOC) represent a crucial component of Northern Hemisphere climate variability. In modelling studies decadal overturning variability has been attributed to the intensity of deep winter convection in the Labrador Sea. This linkage i...

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Bibliographic Details
Published in:Nature Communications
Main Authors: C. W. Böning, P. Wagner, P. Handmann, F. U. Schwarzkopf, K. Getzlaff, A. Biastoch
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Q
Online Access:https://doi.org/10.1038/s41467-023-40323-9
https://doaj.org/article/8bafff3ae90a465788b094da5d1a46ff